| _version_ | 1867169156534632448 |
|---|---|
| author | Eisermann, Hannes |
| author_facet | Eisermann, Hannes |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | Attached data comprise a bathymetric model of central Dronning Maud Land, including the seabed beneath the Nivl Ice Shelf and the Lazarev Ice Shelf, as well as the offshore Astrid Ridge and adjacent parts of the Riiser-Larsen Sea. It gives seabed and ice base depths relative to WGS84 at a resolution of 2.5 km. The bathymetric model is generated by complementing existing topographic data sets - such as seismic data, ice penetrating radar data, and shipborne hydroacoustic data - with the inversion of airborne gravity data towards bathymetry. The airborne gravity data used for the inversion consist of data acquired during aerogeophysical campaigns VISA from the early 2000s and WEGAS from the austral summer of 2009/2010. When citing this model, please also cite the associated manuscript: Eisermann, H., Eagles, G. & Jokat, W. Coastal bathymetry in central Dronning Maud Land controls ice shelf stability. Sci Rep 14, 1367 (2024). https://doi.org/10.1038/s41598-024-51882-2. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_961492 |
| institution | PANGAEA |
| language | en |
| publishDate | 2024 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Bathymetric model beneath Nivl and Lazarev ice shelves, and across Astrid Ridge Eisermann, Hannes Antarctica; Bathymetry; BathymetryModel_cDronningMaudLan; Bed elevation; Dronning Maud Land; Dronning Maud Land, Antarctica; gravity inversion; Ice base elevation; LATITUDE; Lazarev Ice Shelf; LONGITUDE; Model; Nivl Ice Shelf; Polar stereographic projection, X; Polar stereographic projection, Y; water column Attached data comprise a bathymetric model of central Dronning Maud Land, including the seabed beneath the Nivl Ice Shelf and the Lazarev Ice Shelf, as well as the offshore Astrid Ridge and adjacent parts of the Riiser-Larsen Sea. It gives seabed and ice base depths relative to WGS84 at a resolution of 2.5 km. The bathymetric model is generated by complementing existing topographic data sets - such as seismic data, ice penetrating radar data, and shipborne hydroacoustic data - with the inversion of airborne gravity data towards bathymetry. The airborne gravity data used for the inversion consist of data acquired during aerogeophysical campaigns VISA from the early 2000s and WEGAS from the austral summer of 2009/2010. When citing this model, please also cite the associated manuscript: Eisermann, H., Eagles, G. & Jokat, W. Coastal bathymetry in central Dronning Maud Land controls ice shelf stability. Sci Rep 14, 1367 (2024). https://doi.org/10.1038/s41598-024-51882-2. |
| title | Bathymetric model beneath Nivl and Lazarev ice shelves, and across Astrid Ridge |
| topic | Antarctica; Bathymetry; BathymetryModel_cDronningMaudLan; Bed elevation; Dronning Maud Land; Dronning Maud Land, Antarctica; gravity inversion; Ice base elevation; LATITUDE; Lazarev Ice Shelf; LONGITUDE; Model; Nivl Ice Shelf; Polar stereographic projection, X; Polar stereographic projection, Y; water column |
| url | https://doi.org/10.1594/PANGAEA.961492 |